Inner Banda Arc

E245314

The Inner Banda Arc is a volcanic island arc in the Banda Sea region of eastern Indonesia, formed by subduction processes and comprising islands such as Atauro.

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All labels observed (3)

Label Occurrences
Inner Banda Arc canonical 4
Banda volcanic arc 1
Sunda–Banda Arc 1

Statements (43)

Predicate Object
instanceOf geological formation
volcanic island arc
associatedWith Banda Sea Plate
collision of Australian continental margin with island arc
boundedBy Outer Banda Arc
country Indonesia
formedBy convergence of tectonic plates
subduction processes
geologicalAge Cenozoic
geologicalProvince Banda region
hasFeature deep adjacent basins
steep submarine slopes
hasIsland Atauro
Damar
Manuk
Nila
Nusantara volcanic islands (collective)
Romang
Serua
Teon
Tepa
Wetar
hasProcess arc-continent collision
crustal deformation
seismic activity
hasResearchInterest arc-continent collision processes
plate-tectonic evolution of eastern Indonesia
liesNorthOf Timor
liesSouthOf central Banda Sea basin
locatedIn Banda Sea
eastern Indonesia
orientation curved arc
orogeny Banda orogeny
overlies Sunda subduction system
surface form: subducting Australian Plate
partOf Banda Arc
region Maritime Southeast Asia
Southeast Asia
relatedTo Sunda subduction system
surface form: Sunda-Banda Arc system
separates Banda Sea
Timor Sea
tectonicSetting subduction zone
volcanicActivity historically active
volcanismType arc volcanism

Referenced by (6)

Full triples — surface form annotated when it differs from this entity's canonical label.

Atauro islandGroup Inner Banda Arc
Samalas volcano volcanicArcBelt Inner Banda Arc
this entity surface form: Sunda–Banda Arc
Mount Egon mountainRange Inner Banda Arc
Banda Arc contains Inner Banda Arc
Inerie volcano mountainRange Inner Banda Arc
Banda Sea Plate associatedWith Inner Banda Arc
this entity surface form: Banda volcanic arc